固体地球科学 (S)
セッション小記号地球内部科学・地球惑星テクトニクス (IT)
セッション IDS-IT20
タイトル New perspectives on accretion and exhumation processes during oblique plate convergence
タイトル短縮名 Accretion and exhumation processe
開催日時
口頭
セッション
5/25(木) AM1, AM2
現地
ポスター
コアタイム
5/25(木) PM3
オンライン
ポスター
セッション
5/26(金) AM2
代表コンビーナ 氏名 Timothy B Byrne
所属 University of Connecticut
共同コンビーナ1 氏名 Jian-Cheng Lee
所属 Academia Sinica
共同コンビーナ2 氏名 志村 侑亮
所属 産業技術総合研究所
共同コンビーナ3 氏名 Gong-ruei Ho
所属 Academia Sinica, Institute of Earth Sciences
セッション言語 E
スコープ South and East Asia represent one of the most tectonically active regions on Earth. The Pacific, Indo-Australia, and Eurasian plates converge around the Philippine Sea plate, resulting in a wide range of geologically and tectonically complex plate boundaries, including regions of both active and inactive oblique plate convergence. Many of these areas also preserve geologic evidence for subduction of oceanic and continental fragments to high, or ultrahigh pressures (i.e., mantle depths), raising fundamental questions about plate- and outcrop-scale processes. For example, does oblique convergence play a relatively unique role in the generation and/or preservation (i.e., subduction and exhumation) of high-pressure metamorphism? If so, are the accretion and exhumation flow paths truly 3D so plane strain may not apply? Finally, is there a characteristic signature in the rock record that can be used to identify past areas of oblique convergence? Here, we seek oral and poster presentations that bear on the accretion and exhumation processes along modern and ancient plate boundaries associated with either normal or oblique convergence. We also invite discussions of geodynamic models that integrate oblique convergence into a more holistic view of subduction, accretion, and exhumation.
発表方法 口頭およびポスター
共催情報 学協会 -
ジョイント AGU